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- W1521673634 abstract "Pre- and postglacial records of the Indian Ocean are highly influenced by the intensity of monsoon variability. The oxygen isotope records of the Indian Ocean show a two-step deglaciation reflecting two phases of rapid ice melting. A sharp salinity contrast between the pre- and postglaciation is noticed in the Bay of Bengal. Monsoon activity started to increase from 12 000 years; postglacial monsoon variability record show weaker monsoon phases are correlated to the millennial-scale cold spell in the North Atlantic. Monsoon strength, productivity, oxygen minimum zone variability, and denitrification in the Indian Ocean are strongly coupled. Strong monsoon strength, high productivity, and intensified denitrification are noticed in the postglaciation, whereas weak monsoon strength, low productivity, and reduced denitrification are noticed during glaciation." @default.
- W1521673634 created "2016-06-24" @default.
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- W1521673634 date "2013-01-01" @default.
- W1521673634 modified "2023-09-23" @default.
- W1521673634 title "PALEOCEANOGRAPHY, RECORDS | Postglacial Indian Ocean" @default.
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- W1521673634 doi "https://doi.org/10.1016/b978-0-444-53643-3.00301-0" @default.
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